A new remarkable Early Cretaceous nelumbonaceous fossil bridges the gap between herbaceous aquatic and woody protealeans

Dating back to the late Early Cretaceous, the macrofossil record of the iconic lotus family (Nelumbonaceae) is one of the oldest of flowering plants and suggests that their unmistakable leaves and nutlets embedded in large pitted receptacular fruits evolved relatively little in the 100 million years since their first known appearance. Here we describe a new fossil from the late Barremian/Aptian Crato Formation flora (NE Brazil) with both vegetative and reproductive structures, Notocyamus hydrophobus gen. nov. et sp. nov., which is now the oldest and most complete fossil record of Nelumbonaceae. In addition, it displays a unique mosaic of ancestral and derived macro- and micromorphological traits that has never been documented before in this family. This new Brazilian fossil-species also provides a rare illustration of the potential morphological and anatomical transitions experienced by Nelumbonaceae prior to a long period of relative stasis. Its potential plesiomorphic and apomorphic features shared with Proteaceae and Platanaceae not only fill a major morphological gap within Proteales but also provide new support for their unexpected relationships first suggested by molecular phylogenies.

The origin and early radiation of flowering plants are still unclear and remain one of the most enigmatic themes concerning the evolutionary history of vascular plants as a whole 1 . Although the fossil record may help to reduce morphological gaps between living taxa, it is inherently incomplete and may thus miss important evolutionary transitions. Such gaps in evidence for documenting plant evolution can be interpreted either as a consequence of a period with higher evolutionary rates over a short timescale or lower rates of evolution and relative stasis over a long timescale 2 . However, the scarcity of earliest and succeeding forms in fossil records can be also caused by preservational biases, undersampling and low intensity of investigation. Numerous studies of middle paleolatitude floras have significantly reduced the knowledge gaps on Early Cretaceous angiosperms, while those from paleotropical areas, where allegedly flowering plants started to diversify, are still in need of more investigations, especially regarding macrofossils of eudicots, the most diverse angiosperm clade 3,4 . The knowledge gaps on macrofossils in the Early Cretaceous tropics contrast with the substantial and comparatively well-studied microfossil record 5,6 .
The first reports of eudicots date back to the middle Early Cretaceous from circumtethyan areas, i.e., northern Gondwanan and southern Laurasian regions, and suggest that their origin and center of diversification were in northern Gondwana 5,7 . These reports are mainly based on their distinctive tricolpate pollen 7 , but also on macro-and mesofossils thought to be related to basal lineages 8,9 . Among the pieces of evidence, some records are related to Ranunculales and Proteales 8,9 , which are the two earliest diverging lineages of eudicots according to molecular analyses 10  Remarks. Vegetative structures are preserved as reddish-brown replacement fossils and/or impressions with or without a thin iron oxide covering layer. Tissues of the peduncle are also replaced by iron oxide, while the receptacle is a mold with two casts of fruitlets. Clastic material is especially abundant on the rhizome of the holotype, and also in the petiole of the paratype.

Description and remarks.
The holotype is about 50 cm long and 25 cm wide and consists of a rhizome bearing about 30 roots, 13 leaves, and a single aggregate fruit with two visible fruitlets embedded in an enlarged receptacle (Fig. 1). The rhizome is unbranched and about 15 cm long and 1-2 cm wide. The roots are adventitious and up to at least 20 cm long and 0.3 cm wide.
The leaves are petiolate, alternate and simple. Petioles are 12-20 cm long by 0.5-1 cm width. The position of the lamina attachment to the petiole is marginal. Laminar sizes are noto-to mesophyllous, 60 to 95 mm long, and about 60 to 100 mm wide. Laminar shapes are obovate to elliptical, slightly medially asymmetrical to symmetrical, with a length/width (L/W) ratio of about 1. The lamina texture is likely chartaceous. Leaves are unlobed with untoothed margins, obtuse and rounded to slightly cordate bases, and obtuse and rounded to straight-sided apices. The primary venation is palinactinodromous with five primary veins running decurrently basally and bifurcating once or twice distally (Figs. 1C and 2). Naked basal veins are absent, and agrophic veins are present. The midvein is around 0.5-1 mm wide while the lateral primaries are about 0.3-0.8 mm wide. The major secondary venation consists of festooned brochidodromous veins (Figs. 1B and 2B), which are about 0.08-0.14 mm wide. Interior secondaries and intersecondaries are present. The course of the minor secondaries is simple brochidodromous, and a perimarginal vein is absent. The spacing of secondary veins decreases gradually toward the lamina base. Their attachment to the primaries is excurrent and forms a uniform acute angle (about 40°) to the primary veins. Intercostal tertiary veins are mostly opposite percurrent, with convex to sinuous courses (Figs. 1B and 2B). They are obtuse to nearly perpendicular to the midvein with angles decreasing exmedially and are about 0.06-0.09 mm wide. Exterior tertiaries form loops. The quaternary veins are mostly alternate percurrent and about 0.04-0.07 mm wide (Figs. 1B and 2B). Quinternary veins are regular reticulate and about 0.02-0.03 mm wide (Figs. 1B and 3B). The areolation is well developed, 5-to 6-sided (Fig. 3B). Freely ending veinlets are absent. Marginal ultimate venation is looped (Figs. 1B and 2B). Vein density ranges between 7.8-9.9 mm −1 (mean: 9 mm −1 ).
The leaves are bifacial and 0.5 mm thick (Fig. 3A)   www.nature.com/scientificreports/ thick straight anticlinal cell walls and a single papilla per cell (Fig. 3A,D). These papillae are 10-25 µm in diameter and 15-20 µm high (Fig. 3C,D). The lower epidermis is also uniseriate, papillate, and 20-30 µm thick. Its cells are essentially similar in shape to those of the upper epidermis, but slightly smaller and 30-50 µm long and 25-30 µm wide (Fig. 3A,E,F). They also display 3-5 µm thick straight anticlinal cell walls and a single welldeveloped papilla per cell. However, these papillae are also slightly smaller than those of the upper epidermis and 8-25 µm in diameter and 10-15 µm high (Fig. 3E,F). The leaves are amphistomatic with a stomatal density (SD) of about 60-150 mm −2 adaxially, and 100-120 mm −2 abaxially. The stomata are usually 30-35 µm long and 8-30 µm wide, with 15-25 µm long apertures randomly oriented. When the outer periclinal walls of the epidermis are abraded, their guard cells are often kidney-shaped (Fig. 4A,B). The cells in contact with the guard cells are variously shaped, rectangular-polygonal and often asymmetrically in outline, with straight anticlinal cell walls. If these lateral cells belong to the stomatal complexes, the complexes would be (brachy-) paracytic but otherwise anomocytic. In the non-abraded case, the two lateral neighboring cells often partly overlap the guard cells, resulting in a narrow elliptical outline of the stomata in outer surface view (Fig. 3D,F). Compared to the abraded case, the rectangular lateral neighboring cells are often not clearly distinguishable from the ordinary epidermal cells that are characterized by a single papilla on the periclinal walls (Figs. 3D,F and 4). The mesophyll displays a clear dorsiventral organization with an upper/adaxial palisade parenchyma and a lower spongy parenchyma (Fig. 3A). The single cell-layered palisade parenchyma is about 100-150 µm thick, and comprises cylindrical cells with 15-25 widths which display 1-2 µm thick primary walls. The spongy parenchyma is about 300-350 µm thick and consists of more or less globose to irregularly shaped cells that are 20-60 µm in diameter, with 3-4 µm thick primary walls. However, most of these cells are collapsed and their organization is not clear even though some lacunae can be observed. The peduncle of the fruit is 22.5 cm long and 4 mm wide and ends with the hollow mold of the fruit. The fruit is formed by an enlarged ellipsoidal receptacle, which is 2.5 cm long and 4 cm wide (Fig. 1D). It exhibits two globose fruitlets that are about 0.5 cm in diameter and embedded in distinct receptacular pits. Although the distribution of pits on the receptacle remains unclear, the fruit is interpreted as an aggregate derived from an apocarpous gynoecium, where each carpel develops into a fruitlet, likely a nutlet, with an estimated volume of 65 mm 3 on average. No traces or remains of a perianth or other floral/fruit structures are observed below or around the receptacle.
The peduncle shows a pith surrounded by primary xylem bundles and secondary homoxylic (vesselless) xylem without growth rings, and is surrounded by a (peripheral) discontinuous layer interpreted as the remains of the cambial zone (Figs. 5 and 6).
The pith is ovate and 0.6-1.5 mm in diameter (Fig. 5). No tissue is preserved at the center of the pith, but it is unclear whether it was originally hollow or not.
The inner ring of primary xylem comprises ca. 18(19?) xylem bundles, with cells that are unevenly isodiametric and have a 13 to 60 µm wide diameter and a 4-10 µm thick wall (Fig. 5B). Walls of the xylem cells usually have helical and scalariform thickenings (Fig. 6B). Vessel elements are present and appear closer to the pith. They are usually rectangular, upright to drum-shaped, about 40-286 µm long and 17-60 µm wide, and although they are sometimes poorly preserved, scalariform-like pits occur in their side walls and simple perforation plates typically occur in their end walls (Fig. 6A,C).
The homoxylic wood (secondary xylem) consists predominantly of cells interpreted as fibers separated by 19 parenchymatous, homocellular, and usually multiseriate (rarely uniseriate) rays that are about 30-120 µm wide (Fig. 5A). In contrast to the primary xylem cells, the fibers appear more uniform in diameter (15-30 µm), with a 5-10 µm thick wall, a very small lumen, and simple and slit-like pits (Figs. 5A, 6D). Ray cells are also usually more regular, rectangular, and upright, and have a 3-8 µm thick wall with slit-like pit apertures ( Fig. 6A,E,F). Near the pith, they connect with the primary xylem (Fig. 5).
The cambial zone is very poorly preserved. However, it comprises compressed fusiform and elongated cells outside the secondary xylem, from which arise new vascular increments with tracheary elements characterized by scalariform-like pits, including fibers with simple pits (Figs. 5A and 6F,G). These vascular increments are probably derived from anomalous secondary growth.
The anatomy of the petiole also includes vessel elements, which are 65-75 µm in diameter and have 5 µm thick secondary walls with scalariform pits and scalariform perforation plates (Fig. 7). However, in contrast to that the peduncle, it also has abundant aerenchymatous channels (seen as lacunae) and lacks secondary growth.  Phylogenetic analysis. Our cladistic analysis ( Fig. 8) was performed using the matrices by Kvaček et al. 46 and Coiro et al. 47 with the D&E backbone from Endress & Doyle 48 . Our results show that the single most parsimonious position of Notocyamus is within Proteales, as sister to Nelumbo (Nelumbonaceae), and supported by synapomorphies of the two taxa within Proteales, such as the lack of freely ending veinlets (CH14), solitary flowers (CH43), and the presence of pits in receptacle bearing individual carpels (CH52). The herbaceous habit (CH1) and anomocytic stomata (CH37) are also shared between them and could equally be synapomorphies among Proteales since all other taxa (including Sabiaceae) are woody and predominantly possess paracytic and laterocytic stomata (modified to anomocytic in some Platanaceae and Sabiaceae) 49,50 . However, the point on the tree at which these shared character states arose is ambiguous. Chloranthoid teeth (CH36) are a plesiomorphic character widespread in basal eudicots 12 , and their loss is a synapomorphy of Proteales (modified to platanoid teeth in Platanaceae). However, Notocyamus and Nelumbo still differ in the scoring of cambium (CH6), vessel perforation (CH09), leaf shape (CH30), and base of blade (CH33), and by the presence of paracytic stomata (CH37). In Proteales, loss of cambium (CH6) and evolution of peltate leaves (CH33) are autapomorphies of Nelumbo.
The position sister to Magnoliales and Laurales is one step less parsimonious and supported by the fiber pitting (CH10), and the presence of solitary flowers (CH43) (common in Magnoliales). However, they differ markedly from Notocyamus and Nelumbo in having freely ending veinlets (CH14) (lacking only in Lauraceae), pinnate major venation (CH31) (modified to palmate in a few Laurales), and in lacking pits in the receptacle (CH52).
We also found an alternative two step less parsimonious position in Proteales with Notocyamus sister to Platanaceae + Proteaceae. This position is supported by mixed scalariform and simple vessel perforation plates (CH9), but it requires two origins of freely ending veinlets (CH14), solitary flowers (CH43), and receptacle with carpel-bearing pits (CH52), or one origin of these features followed by a reversal in Platanus and Proteaceae.
Three additional two step less parsimonious positions were retrieved among magnoliids, with Notocyamus sister to either Piperales or Galbulimima in Magnoliales, and monocot. The alternate position as sister to Piperales is supported by palmate venation (CH31) but requires one more step in each of these characters (CH14, CH43, CH52) than the position with Nelumbo. The position sister to Galbulimima is supported by vessel perforation (CH9) and fiber pitting (CH10) but also requires one more step in several characters, in this case due to the

Discussion
Age of the fossil and paleogeographical implications. Notocyamus is described from the late Barremian?/Aptian of Brazil and is thus older than the previously oldest representative of its clade, i.e., Nelumbites extenuinervis from the middle to upper Albian of USA 18,19 , but also than isolated leaves of Nelumbites from Kazakhstan 16 . Its older age is consistent with the fact that several of its morphological characters are more plesiomorphic than those of Albian Nelumbites and extant Nelumbo. In addition, molecular dating indicates that the divergence time of Nelumbonaceae and Platanaceae is around 83 to 123 Ma 14,19,51-53 . These older age estimates are very close to the first pieces of evidence from the fossil record of this family even though their divergence time could still be earlier 14,54 .
Our findings also raise questions on the paleogeographic origin of the family since until our study, distributions of all previous fossil records suggested an origin of Nelumbo in Laurasian mid-latitudes 25 . Also, Ramírez-Barahona et al. 55 suggest that the ancestral biome of Nelumbonaceae is most likely coupled with more temperate than tropical climates. However, whether their initial evolutionary history is linked to Laurasian midlatitude areas and ancestral temperate biomes 25,55 , or not, remains unclear. Our report preliminarily suggests that the initial evolution of Nelumbonaceae may have occurred in northern Gondwanan low-latitude areas under a seasonal tropical climate since Notocyamus is currently the oldest record of this family and displays traits interpreted as ancestral for the family. This new Brazilian fossil also adds data to postulate that the paleoequatorial tropical areas were an important center of early diversification of basal eudicots in the Early Cretaceous before reaching mid-latitude areas, where they became widespread from the Albian onwards. This hypothesis was discussed by Doyle 5 based on fossil pollen records and is currently being reinforced by an increasing number of macrofossils of basal eudicots described from the Crato Formation 8 , but also by evidence from tricolpate pollen already reported in this same lithostratigraphic unit 32 .
Morphological adaptation for an aquatic habitat. In terms of habit and morphology, Notocyamus resembles living Nelumbonaceae and implies a paleoecology adapted to similar aquatic conditions (see reconstruction, Fig. 9). In contrast to the woody habit of the other Proteales, fossil and extant members of the family share the same rhizomatous habit 26,56 (Fig. 1A). In addition, the presence of long petioles in both Notocyamus (Figs. 1A and 2A) and living Nelumbonaceae enables the laminae to reach the water surface and beyond. In Nelumbo, this elongation is conditioned to water depth and flooding events, and this adaptive response is medi- www.nature.com/scientificreports/ ated by ethylene gas flowing through aerenchyma 57,58 . Such a specialized tissue with numerous air chambers is also present in the petiole of Notocyamus and living Nelumbonaceae. It also typically occurs in plants growing in aquatic-related environments under anoxic conditions, not only to allow sufficient oxygen levels to maintain respiration through gas canals but also to improve their mechanical support [58][59][60] . The leaf epidermises of Notocyamus and living Nelumbo are also essentially similar by having anomocytic stomata (Fig. 3D,F) with similar density average values on the upper surfaces 15,61 , and dense papillae with superhydrophobic properties (Fig. 3), producing the famous "Lotus effect" 62 . The water-repellent nature of leaves facilitates water and dirt particles removal on the leaf surface and ensures stomata function and gas exchanges 63,64 . Such water-repellent leaf surfaces are especially common in herbaceous plants living in disturbed and wetland environments 63 . The only notable micromorphological difference is that the leaf of Notocyamus also bears likely (brachy-) paracytic stomata and distinct epidermal papillae on both sides, whereas those of Nelumbo are exclusively anomocytic and almost entirely epistomatic with papillae present only on their adaxial (upper) surfaces 61,[65][66][67] . It suggests the development of emergent leaves in Notocyamus and subsequent exaptation of the Lotus effect in peltate leaves of Nelumbonaceae. Such emergent and amphistomatic leaves, despite being rare in Nelumbo, are also well-documented in other aquatic plant lineages 59 . In addition, the relatively high leaf vein density (ca. 9 mm −1 ) in Notocyamus may support a higher water supply capacity leading to a better leaf hydraulic conductance and consequently higher photosynthetic and transpiration rates [68][69][70] . As in living Nelumbo species, it would probably also allow establishment in sunny habitats under conditions of high temperatures.
Both Notocyamus and living Nelumbonaceae also display a typically enlarged floral receptacle that develops into an aggregate fruit with several nutlets embedded in pits 26,71 (Fig. 1A,D). This kind of fruit is adapted to float in aquatic habitats and disperses its diaspores passively by hydrochory 13,72 . In addition, the reproductive organs associated with though not attached to the leaves of Nelumbites extenuinervis Upchurch, Crane et Drinnan, and Nelumbo puertae Gandolfo et Cuneo also share an enlarged receptacle with fruitlets 18,23 .  73,74 , suggesting that these traits were homologous in all these groups. This similarity is also seen in some Cretaceous platanoid leaves assigned to Credneria Zenker and Platanus, which also display palinactinodromous venation 75 . Notocyamus often shares the obovate to elliptical leaf shapes (Figs. 1A and 2A) with these fossils, and related lineages such as Proteaceae and Sabiaceae, which contrasts with the leaves of Nelumbo and its younger fossil relatives, indicating that Nelumbonaceae passed through this morphological stage before having orbicular leaves 20 .
The presence of paracytic and anomocytic stomata in Notocyamus may strengthen the concept of its mosaic of ancestral and derived characters. Since almost all woody protealeans vary between paracytic and laterocytic stomata, and Nelumbo has exclusively anomocytic stomata, this may suggest that Notocyamus is in a transitional form between ancestral (paracytic stomata) and derived (anomocytic stomata) anatomical traits.
If the leaf architecture of Notocyamus is considered to be plesiomorphic for the family, Notocyamus can be interpreted as a first evolutionary step towards Nelumbo. Nelumbites 18 , from the Albian, can be interpreted as a second evolutionary step. Its leaf blade is already peltate, but eccentric, its primary venation is actinomorphic but comprises only a few primaries (< 10), and its lamina is orbicular, displaying a basal indentation reminiscent of the sometimes-cordate leaf bases of Notocyamus. Exnelumbites 20 , from the Campanian-Maastrichtian, which can be interpreted as a third evolutionary step, is already centrally peltate but displays 12-13 primaries and surprisingly bears chloranthoid teeth. Paleonelumbo, from the Paleocene, is another genus with distinct leaf architecture: although its leaves are centrally peltate, they are quite distinct from those of Nelumbo in being lobed and having 10-15 primary veins 15,20 . Nelumbago, also from the Paleocene, is, however, very similar to extant and extinct species of Nelumbo in terms of foliar architecture and can therefore be interpreted as the next to last evolutionary step in having centrally peltate and entire-margined leaves with > 20 bifurcating primary veins but still no central disk 15,20 . All extinct and extant Nelumbonaceae cited above suggest that peltation of their leaves did not evolve until a certain time after the divergence of Nelumbonaceae.
Despite differing significantly in its leaf architecture by having a distinct primary venation type, Notocyamus exhibits a special similarity to Nelumbo in lacking the freely ending veinlets. This leaf character is rare in basal eudicots and occurs only in Nelumbonaceae in Proteales. In addition, Notocyamus and Nelumbo share the same entire-margined leaf blades, bifurcating primary venation, festooned brochidodromous secondary venation, tertiary and quaternary veins with mixed course, and six-sided areolae 15,20 .
In terms of reproductive structures, Notocyamus and other Nelumbonaceae both produce single flowers sharing an apomorphic feature: carpel-bearing pits in the receptacle. The shape of the floral receptacle appears to have evolved from ellipsoidal in Notocyamus, to slightly conical in Nelumbites extenuinervis and Nelumbo puertae 18,23 , culminating in the well-known obconical shape in Nelumbo. Although the reproductive organs of both Notocyamus and Nelumbo are borne on long peduncles (Fig. 1A), their peduncles are quite distinct anatomically 76 , because only Notocyamus has secondary xylem produced by a vascular cambium, as in other members of Proteales, which are woody plants. Interestingly, the secondary growth did not disappear in the nelumbonaceous line until some time after its divergence from other Proteales. In its peduncle, Notocyamus bears several water-conducing cells in each primary xylem bundle, and in the secondary xylem (wood) nonconductive cells (fibers with lignified walls) occur (Figs. 5 and 6). Most woody tissues of Notocyamus consist of fibers with simple and slit-like pits (Figs. 5 and 6D). These structures also occur in the most closely related lineages: Platanaceae usually have fiber tracheids with bordered and simple pits 77 , most genera of the Proteaceae have libriform fibers with simple and bordered pits 78 , and the majority of Sabiaceae taxa have libriform fibers with vestigial bordered pits 79 . Concerning the type of vessel perforation in the primary xylem, Notocyamus displays the same combination of simple and scalariform vessel perforation plates as Platanaceae, Proteaceae, and Sabiaceae, suggesting that this state could be a synapomorphy of the Proteales, but Nelumbo may represent a reversal of this trend. The specialization of vessel perforation plates from scalariform to simple has long been interpreted as derived and occurred several times in different lineages 80,81 . Overall importance for evolution of Proteales and conclusions. Fossils of Proteales show that members of this group already inhabited contrasting environments during the Early Cretaceous, with terrestrial woody Platanaceae and aquatic herbaceous Nelumbonaceae. Unfortunately, macrofossils of Proteaceae and Sabiaceae are sporadic in the Cretaceous and better recognized and described in Cenozoic floras 9 . However, fossil representatives of Nelumbonaceae and Platanaceae confirm that huge differences in gross morphology already existed between Cretaceous members of these families (e.g., Nelumbites, and Sapindopsis, respectively). In addition, the fossils show that the living Platanus and Nelumbo are similar to some of their Early Cretaceous members, and that these clades thus likely experienced early rapid morphological evolution followed by a long period of relative stasis.
Besides our results from cladistics supporting the position of Notocyamus as a stem-relative of Nelumbonaceae, the fossils not only push back the minimum age of the appearance of the lotus lineage to at least the early Aptian but also shed light on the morphological evolution of its vegetative and reproductive traits. Despite the putative stasis previously reported in this family, their stem lineages may still have undergone considerable morphological changes throughout geological time. In addition, our report surprisingly provides new lines of evidence that the Compared to other extinct nelumbonaceous fossils, Notocyamus displays a new and unique mosaic of ancestral states shared with Platanaceae and Proteaceae, and derived states shared with Nelumbo, and clarifies important evolutionary steps of Nelumbonaceae and Proteales as a whole. Thus, Notocyamus ideally fills the morphological gap between aquatic Nelumbonaceae and their most recent common ancestor with woody Proteales, and can therefore be seen as one of those "missing links" that are rarely preserved in the fossil record.

Methods
Fossil analysis. The fossils were studied using a Leica Wild M10 microscope equipped with a Leica DFC 425 camera. Overview images were taken with a Canon 250D camera. Vegetative structures (leaves, petiole, and peduncle) of Notocyamus exhibit anatomical details preserved by iron oxide replacement of tissues. These details were observed in a high vacuum with a Scanning Electron Microscope (SEM) (Carl Zeiss EVO 50 and EVO LS 10, Germany). For SEM analyses, pieces of leaves, petiole and peduncle were removed from the specimen, mounted on stubs, and coated with gold for four minutes with a Polaron SC7640 sputter coater. Photographs of fossils were edited with Adobe Photoshop software.
Leaf architecture. The description of leaf architecture follows Ellis et al. 45 .
Leaf width inferences. The leaf width measurements of Notocyamus (holotype) were inferred from leaves with at least half the lamina preserved (including folded leaves), multiplying the distance from the midvein to the lamina margin by two supposing a symmetrical lamina shape. They were used to estimate the laminar size, L:W ratio, and leaf shape.
Vein and stomata density measurements. The vein density (mm of vein per mm 2 ) of Notocyamus was calculated based on an SEM image (Fig. 3B) that best shows the length of quinternary veins. The measurements were made using the program ImageJ (https:// imagej. nih. gov/). The stomatal density (SD) on leaves of Notocyamus was calculated using seven SEM images from different leaf pieces on both adaxial and abaxial sides. The presence of stomata was counted on squares of 0.12 to 0.3 mm 2 to calculate the stomata density in mm −2 .
Fruitlet volume measurements. The volume of fruitlets was estimated based on the formula V = 4/3πr 3 , following Tiffney 82 .
Thin sections. Petrographic thin sections of the peduncle were made in the three standard sections used for studying wood anatomy: transversal, radial, and tangential (sensu Jones and Rowe 83 ). Slides were analyzed and photographed using a Zeiss light microscope (Axioscope 5) coupled to a Canon 60D camera.
Cladistic analysis. The phylogenetic analysis was performed by adding the fossil as a new taxon to the morphological data set from Kvaček et al. 46 and Coiro et al. 47 with character states presented in Supplementary Information, using the D&E backbone constraint tree 48 . The relative parsimony of all positions of the fossil was evaluated using Mesquite 3.61 84 , and the number of required character state changes (steps) in each alternative tree was recalculated. All characters were unordered and equally weighted. Updated age estimation for the Crato Formation. The Crato Formation, the second lithostratigraphic unit from the base of the Santana Group, has been repeatedly dated as upper Aptian age based on palynological evidence 32 . By contrast, new results of Melo et al. 34 , Barreto et al. 36 and Arai & Assine 85 consistently revealed an upper Aptian age for the Romualdo Formation, the uppermost unit of the Santana Group, based on relative and absolute dating methods. In addition, the Ipubi Formation, which underlies the Romualdo Formation, contains two important layers for age estimation, the black shale at its base and the evaporite layer soon above. Lúcio et al. 33 dated this evaporite layer by Re-Os isotope studies as 123 ± 3.5 Ma (126.5 to 119.5 Ma). Besides, isotope and organic geochemistry of this black shale provides strong evidence that it was deposited during the global Ocean Anoxic Event OAE-1a 35 . The numerical age of the base of OAE-1a, called the Selli event, is ca. 119-120 Ma 86 . Thus, the Crato Formation, underlying the Ipubi Formation, is at least older than 120 Ma, which is not far above the base of the Aptian, or even older if there was a hiatus between the formations 27 .
Since 2022, the updated international chronostratigraphic chart shows a new age for the base of the Aptian (121.4 Ma instead of 125 Ma), which is correlated with a short-lasting magnetostratigraphic zone 87 .
According to Neumann et al. 29 , the C6 carbonate unit of the Crato Formation could represent a period of up to 0.5 Ma. Altogether, the Crato limestones C1-C6 could likely represent several million years, which would extend its absolute age range towards the upper Barremian. However, such a fundamental change in the age of the Crato Formation needs to be supported by additional unambiguous evidence in future publications.

Data availability
All data analyzed during the current study are included in this published article and its supplementary information file.